Optimising global landscape evolution models with 10Be

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Optimising global landscape evolution models with ¹⁰Be ; day:08 ; month:11 ; year:2022 ; pages:1-32 ; extent:32
Earth surface dynamics discussions ; (08.11.2022), 1-32 (gesamt 32)

Creator: Ruetenik, Gregory
Jansen, John D.
Val, Pedro
Ylä-Mella, Lotta

DOI: 10.5194/esurf-2022-54

URN: urn:nbn:de:101:1-2022111004232623725995

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:33 AM CEST

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Ruetenik, Gregory
Jansen, John D.
Val, Pedro
Ylä-Mella, Lotta

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Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Cosmogenic 10Be in pyroxene: laboratory progress, production rate systematics, and application of the 10Be–3He nuclide pair in the Antarctic Dry Valleys

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Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

Evolution von Datenmodellen : Relational ... geschachtelt (NF2) relational ... objektorientiert?

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH4+–Na+–Ca2+–K+–Mg2+–SO42−–NO3−–Cl−–H2O system based on ISORROPIA II

Simulations of 7Be and 10Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

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Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Cosmogenic 10Be in pyroxene: laboratory progress, production rate systematics, and application of the 10Be–3He nuclide pair in the Antarctic Dry Valleys

Technical note: Accelerator mass spectrometry of 10Be and 26Al at low nuclide concentrations

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Relationship between meteoric 10Be and NO3− concentrations in soils along Shackleton Glacier, Antarctica

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Optimising global landscape evolution models with <sup>10</sup>Be

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Other Objects (12)

Optimising global landscape evolution models with <sup>10</sup>Be

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Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

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Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Optimising global landscape evolution models with <sup>10</sup>Be

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Cosmogenic <sup>10</sup>Be in pyroxene: laboratory progress, production rate systematics, and application of the <sup>10</sup>Be–<sup>3</sup>He nuclide pair in the Antarctic Dry Valleys

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Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

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Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Optimising global landscape evolution models with <sup>10</sup>Be

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Cosmogenic <sup>10</sup>Be in pyroxene: laboratory progress, production rate systematics, and application of the <sup>10</sup>Be–<sup>3</sup>He nuclide pair in the Antarctic Dry Valleys

Technical note: Accelerator mass spectrometry of <sup>10</sup>Be and<sup> 26</sup>Al at low nuclide concentrations

Technical note: Accelerator mass spectrometry of <sup>10</sup>Be and <sup>26</sup>Al at low nuclide concentrations

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Evolution von Datenmodellen : Relational ... geschachtelt (NF<sup>2</sup>) relational ... objektorientiert?

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Optimising global landscape evolution models with <sup>10</sup>Be

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Other Objects (12)

Optimising global landscape evolution models with <sup>10</sup>Be

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Cosmogenic <sup>10</sup>Be in pyroxene: laboratory progress, production rate systematics, and application of the <sup>10</sup>Be–<sup>3</sup>He nuclide pair in the Antarctic Dry Valleys

Technical note: Accelerator mass spectrometry of <sup>10</sup>Be and<sup> 26</sup>Al at low nuclide concentrations

Technical note: Accelerator mass spectrometry of <sup>10</sup>Be and <sup>26</sup>Al at low nuclide concentrations

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Evolution von Datenmodellen : Relational ... geschachtelt (NF<sup>2</sup>) relational ... objektorientiert?

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Optimising global landscape evolution models with <sup>10</sup>Be

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Cosmogenic <sup>10</sup>Be in pyroxene: laboratory progress, production rate systematics, and application of the <sup>10</sup>Be–<sup>3</sup>He nuclide pair in the Antarctic Dry Valleys

Technical note: Accelerator mass spectrometry of <sup>10</sup>Be and<sup> 26</sup>Al at low nuclide concentrations

Technical note: Accelerator mass spectrometry of <sup>10</sup>Be and <sup>26</sup>Al at low nuclide concentrations

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Evolution von Datenmodellen : Relational ... geschachtelt (NF<sup>2</sup>) relational ... objektorientiert?

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

Optimising global landscape evolution models with <sup>10</sup>Be

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Cosmogenic <sup>10</sup>Be in pyroxene: laboratory progress, production rate systematics, and application of the <sup>10</sup>Be–<sup>3</sup>He nuclide pair in the Antarctic Dry Valleys

Technical note: Accelerator mass spectrometry of <sup>10</sup>Be and<sup> 26</sup>Al at low nuclide concentrations

Technical note: Accelerator mass spectrometry of <sup>10</sup>Be and <sup>26</sup>Al at low nuclide concentrations

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Evolution von Datenmodellen : Relational ... geschachtelt (NF<sup>2</sup>) relational ... objektorientiert?

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Simulations of <sup>7</sup>Be and <sup>10</sup>Be with the GEOS-Chem global model v14.0.2 using state-of-the-art production rates

Relationship between meteoric <sup>10</sup>Be and NO<sub>3</sub><sup>−</sup> concentrations in soils along Shackleton Glacier, Antarctica

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Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

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